Calculator · Structural Mechanics

Plane Stress Transformation Calculator

The same stress state looks different on differently oriented faces. Rotating the element counter-clockwise by θ redistributes the state between normal and shear components while leaving the sum σx + σy unchanged.

Stress state

σ is tensile positive. τxy acts on the +x face in the +y direction. θ is a counter-clockwise rotation of the axes in physical space.

Elements

xyσy = -20 MPaσx = 80 MPaτ = 30 MPa
Reference element. Tensile normal stress pulls outward, compressive pushes inward; a positive τ acts on the +x face in the +y direction.
xyσy′ = -20.98 MPaσx′ = 80.98 MPaτ = -28.3 MPa
Element rotated 30° counter-clockwise. Tensile normal stress pulls outward, compressive pushes inward; a positive τ acts on the +x′ face in the +y′ direction.

Transformed components

Rotation θ30°
σx′80.981 MPa
σy′-20.981 MPa
τx′y′-28.301 MPa
Invariant σx + σy60 MPa → 60 MPa
Maximum in-plane shear τmax58.31 MPa

Open in the Lab

Open in Stress Transformation Lab

The Lab sweeps θ with both elements and Mohr's circle updating together.

Technical reference

σx′ = (σx+σy)/2 + (σx−σy)/2 · cos 2θ + τxy · sin 2θ

σy′ = (σx+σy)/2 − (σx−σy)/2 · cos 2θ − τxy · sin 2θ

τx′y′ = −(σx−σy)/2 · sin 2θ + τxy · cos 2θ

σx, σy
normal stresses on the reference faces, tensile positive[Pa]
τxy
shear on the +x face acting in the +y direction[Pa]
θ
counter-clockwise rotation of the axes in physical space[rad]

Everything depends on 2θ, so the state repeats every 180° of physical rotation — a face and the face 180° away carry identical stresses.

σx + σy is invariant under rotation. If the two sums differ in the table above by more than rounding, the inputs are not a valid plane-stress state.

This is PLANE stress: σz = 0 on the free surface. The third principal stress is zero and is not in-plane, which matters when the maximum absolute shear is wanted rather than the maximum in-plane shear.

Assumptions

  • · Plane stress: one face of the element is free, so σz = τxz = τyz = 0.
  • · θ is a rotation of the observation axes, not a deformation of the material.
  • · Static, linear-elastic conditions; the transformation itself is pure equilibrium and holds for any material.

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